Simulation of Magnesium Oxide Behavior under High-Energy Impact Научная публикация
Журнал |
Combustion, Explosion and Shock Waves
ISSN: 0010-5082 |
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Вых. Данные | Год: 2024, Том: 60, Страницы: 260-268 Страниц : 9 DOI: 10.1134/S0010508224020126 | ||
Ключевые слова | equation of state of matter, phase transition, magnesium silicates, magnesium oxide | ||
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Организации |
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Реферат:
Magnesium oxide is one of many important materials that comprise the mantles of terrestrial planets. In this regard, its properties at high temperatures and pressures reflect the nature of the planetary interior. Shock wave loading of magnesium oxide with account for polymorphic phase transition in a pressure range of 325–400 GPa is numerically simulated using a thermodynamic equilibrium model. The parameters of the consistent equation of state for high- and low-pressure magnesium oxide phases (MgO I and MgO II) are determined. The thermodynamic parameters of these phases are simulated. The Hugoniots of single and double compression are constructed in a range of 1–1000 GPa, and the following parameters are calculated: heat capacity along the normal isobar, entropy as a function of temperature, and temperature along the Hugoniot. The simulation results are verified using data from experiments and calculations of other authors.
Библиографическая ссылка:
Maevskii K.K.
Simulation of Magnesium Oxide Behavior under High-Energy Impact
Combustion, Explosion and Shock Waves. 2024. V.60. P.260-268. DOI: 10.1134/S0010508224020126 WOS
Simulation of Magnesium Oxide Behavior under High-Energy Impact
Combustion, Explosion and Shock Waves. 2024. V.60. P.260-268. DOI: 10.1134/S0010508224020126 WOS
Оригинальная:
Маевский К.К.
МОДЕЛИРОВАНИЕ ПОВЕДЕНИЯ ПЕРИКЛАЗА ПРИ ВЫСОКОЭНЕРГЕТИЧЕСКОМ ВОЗДЕЙСТВИИ
Физика горения и взрыва. 2024. Т.60. №2. С.127-135. DOI: 10.15372/FGV2022.9278 РИНЦ OpenAlex
МОДЕЛИРОВАНИЕ ПОВЕДЕНИЯ ПЕРИКЛАЗА ПРИ ВЫСОКОЭНЕРГЕТИЧЕСКОМ ВОЗДЕЙСТВИИ
Физика горения и взрыва. 2024. Т.60. №2. С.127-135. DOI: 10.15372/FGV2022.9278 РИНЦ OpenAlex
Идентификаторы БД:
Web of science: | WOS:001333859900002 |
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